The model for
source-receptor distances of the order of kilometers
was evaluated with data derived from two tracer experiments
conducted during August and December of 2001 at Barrio
Logan, San Diego. |
Observed turbulent intensities vary by
less
than 20% in the vertical in the boundary layer |
|
Model performance when initial
spreads
are taken to be zero
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|
|
|
|
|
Better model performance
when initial
horizontal spread is taken to be 50m
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It's necessary
to account for initial plume
spread caused by building effects to explain concentrations on the 200m
and 500m arcs. |
Model performance based on turbulent intensities
averaged over the entire field study is almost as well as
the
model performance using experiment specific meteorology
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|
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Venkatram, A., Isakov,
V., Pankratz, D., and
Yuan, J., 2005: Relating plume spread to meteorology in urban areas. Atmospheric Environment, 39(2), 371-380
Venkatram, A., Isakov, V., Yuan, J., Pankratz, D., 2004: Modeling
dispersion at distances of meters from urban sources. Atmospheric
Environment, 38, 4633-4641
Venkatram, A.,
Isakov, V., Pankratz, D., Heumann, J., and Yuan, J., 2004: The analysis of data
from an urban dispersion experiment. Atmospheric Environment, 38(22),
3647-3659
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